Phosphorus source seems to be another important factor affecting phosphorus movement in
soils and thus the efficacy of fertigation. Stanberry et al.
(124), using radioautographs to trace P32
movement in Superstition sand, noted that phosphorus from phosphoric acid and monocalcium
phosphate moved vertically across the length of the photographic film (20 cm) compared to dicalcium
phosphate and tricalcium phosphate, which showed negligible movement. Lauer
(122)
reported that sprinkler-applied monoammonium phosphate, urea phosphate, and phosphoric acid
showed similar movement in soils. However, ammonium polyphosphate penetrated only to 60 to
70% of the depth of the other sources. Rauschkolb
(125) reported that glycerophosphate moved
slightly farther than orthophosphate when injected through a trickle-irrigation system but phosphorus
from both sources moved a sufficient distance into the root zone such that phosphorus availability
was adequate for tomatoes. O’Neill
(126) reported that orthophosphoric acid applied in the
irrigation water for trickle-irrigated citrus (Citrus spp. L.) was delivered to a greater soil volume
than triple superphosphate applied directly below the emitter. The phosphoric acid also lowered the
pH of the irrigation water sufficiently to eliminate clogging problems associated with the precipitation
of phosphorus in the irrigation lines.